In recent decades, the land-ocean aquatic continuum, commonly defined as the interface, or
transition zone, between terrestrial ecosystems and the open ocean, has undergone …

Accurate probabilistic seismic hazard analysis requires a good knowledge of the recurrence
parameters of the strongest earthquakes in a region. Due to the typical short temporal span …

In regions with moderate seismicity and large intervals between strong earthquakes,
paleoseismological archives that exceed the historical and instrumental timescale are …

High‐Alpine regions are prone to a large variety of geohazards, among which earthquakes
have the strongest impact on landscape and local population. Historic records indicate a …

Along continental margins with rapid sedimentation, overpressure may build up in porous
and compressible sediments. Large-scale release of such overpressure has major …

Slow-moving subaqueous landslides (SMSL) have been recognised in many studies from
seafloor bathymetric and seismic data, based on shared morphological characteristics with …

The Storegga tsunami (c. 8150 cal BP) is geologically well attested from various isolation
basins across the west Norwegian coast. Ascertaining the impact it had upon the Mesolithic …

Four decades of studies on pristine Baffin Island fjords are summarized with respect to
sediment redistribution processes and resulting deposits. Sediment fill in these fjords …

In this study, identified mass transport deposits (MTDs) in previously analyzed as well as
new sediment cores and seismic profiles from 22 fjord systems and six lakes in west and mid …

Petermann Fjord is a deep (> 1000 m) fjord that incises the coastline of north-west
Greenland and was carved by an expanded Petermann Glacier, one of the six largest outlet …